the community land model - biogeophysics...the community land model - biogeophysics keith oleson...

The Community Land Model - Biogeophysics

Keith Oleson NCAR Earth System Laboratory

Climate and Global Dynamics Division Terrestrial Sciences Section

oleson@ucar.edu

Thanks to Dave Lawrence (co-chair LMWG)

NCAR is sponsored by the National Science Foundation

Outline

• Why is the land surface an important component of the climate system?

• Role of a land surface model in an Earth System Model

• Main features of CLM

– Structural aspects (surface/input datasets)

– Component submodels

• Biogeophysics (SP)

• Biogeochemistry (Carbon-Nitrogen(CN), Dynamic Vegetation (CNDV), Biogenic Volatile Organic Compounds (BVOCs), Dust)

How do we test, evaluate and improve CLM?

Why the focus on land

What a land model within an Earth System Model that consists of so many important pieces?

distinguishes

The land is a critical interface

through which climate, and climate change impacts humans and ecosystems

and

through which humans and ecosystems can effect global environmental and climate change

Observed terrestrial change

Deforestation

Permafrost degradation (Akerman, 2008)

NH snow cover anomaly (Rutger’s Global Snow Lab)

Arctic greening (Bunn et al. 2007)

Water resources: When will Lake Mead go dry?

Milly et al., 2005

Barnett and Pierce 2008

% Change in Runoff by 2050 (A1B)

Soil moisture – Precipitation feedback

How much does a precipitation-induced soil moisture anomaly influence the overlying atmosphere and thereby the evolution of weather and the generation of precipitation?

Photo by D. Fritz

Land-atmosphere interactions

GLACE: To what extent does soil moisture influence the overlying atmosphere and the generation of precipitation?

Koster et al., 2004; IPCC

How does the representation of land-atmosphere interactions affect simulation of droughts, floods, extremes?

Lakes drain, soil dries

Arctic warming

Arctic climate-change feedbacks

Enhanced nitrogen

CO2 efflux

Global warming

CH4 efflux

Microbial activity

increases

Shrub growth

Expanded wetlands

Carbon sequester

Adapted from McGuire et al., 2006

Permafrost warms and

thaws

Arctic runoff increases

Why the focus on land

– exchanges of momentum, energy, water vapor, CO2, dust, and other trace gases/materials between land surface and the overlying atmosphere (and routing of runoff to the ocean)

– states of land surface (e.g., soil moisture, soil temperature, canopy temperature, snow water equivalent, C and N stocks in veg and soil)

– characteristics of land surface (e.g., soil texture, surface roughness, albedo, emissivity, vegetation type, cover extent, leaf area index, and seasonality)

The role of the land model in an Earth System Model

Absorbed solar D

iffu

se s

ola

r

Do

wn

we

llin

g

lon

gw

ave

Reflected solar

Em

itte

d

lon

gw

ave

Se

nsi

ble

he

at f

lux

La

ten

t he

at f

lux

ua 0

Momentum flux Wind speed

Soil heat flux

Evaporation

Melt

Sublimation

Throughfall

Infiltration Surface

runoff

Evaporation

Transpiration

Precipitation

Heterotrophic respiration

Photosynthesis

Autotrophic respiration

Litterfall

N uptake

Vegetation C/N

Root litter Soil C/N

N mineralization

Fire

Surface energy fluxes Hydrology

Biogeochemical cycles

SCF

Aerosol deposition

Bedrock

Soil (sand, clay, organic)

Unconfined aquifer Sub-surface

runoff

Aquifer recharge

Phenology

BVOCs

Water table

Soil

Dust

Saturated fraction

N dep N fixation

Denitrification N leaching

Glacier

Lake

River Routing

Runoff

River discharge

Urban

Land Use Change

Wood harvest

Disturbance

Vegetation Dynamics

Growth

Competition Wetland

Figure 1: Lawrence et al., Journal Advances Modeling Earth Systems, 2011

The role of CLM in CESM: Land to Atmosphere

1Latent heat flux vap v gE Eλ λ+ W m-2

Sensible heat flux v gH H+ W m-2

Water vapor flux v gE E+ mm s-1

Zonal momentum flux xτ kg m-1 s-2

Meridional momentum flux yτ kg m-1 s-2

Emitted longwave radiation L ↑ W m-2

Direct beam visible albedo v i sI µ↑ -

Direct beam near-infrared albedo n i rI µ↑ -

Diffuse visible albedo v i sI ↑ -

Diffuse near-infrared albedo n i rI ↑ -

Absorbed solar radiation S

W m-2

Radiative temperature radT K

Temperature at 2 meter height 2mT K

Specific humidity at 2 meter height 2mq kg kg-1

Snow water equivalent snoW m

Aerodynamic resistance amr s m-1

Friction velocity u∗ m s-1 2Dust flux jF kg m-2 s-1

Net ecosystem exchange NEE kgCO2 m-2 s-1

The role of CLM in CESM: Atmosphere to Land

1Reference height atmz′ m

Zonal wind at atmz atmu m s-1

Meridional wind at atmz atmv m s-1

Potential temperature atmθ K

Specific humidity at atmz atmq kg kg-1

Pressure at atmz atmP Pa

Temperature at atmz atmT K

Incident longwave radiation atmL ↓ W m-2 2Liquid precipitation rainq mm s-1 2Solid precipitation snoq mm s-1

Incident direct beam visible solar radiation atm visS µ↓ W m-2

Incident direct beam near-infrared solar radiation atm nirS µ↓ W m-2

Incident diffuse visible solar radiation atm visS ↓ W m-2

Incident diffuse near-infrared solar radiation atm nirS ↓ W m-2

Carbon dioxide (CO2) concentration ac ppmv 3Aerosol deposition rate spD kg m-2 s-1 4Nitrogen deposition rate _ndep sminnNF g (N) m-2 yr-1

At each timestep the land scheme solves …

• Surface energy balance

– S↓ + L↑ = S↑ + L↓ + λE + H + G

S↓, S↑ are down(up)welling solar radiation,

L↑, L↓ are up(down)welling longwave radiation,

λ is latent heat of vaporization, E is evaporation,

H is sensible heat flux, and G is ground heat flux

• Surface water balance

– P = ES + ET + EC + Rsurf + RSub-Surf + (∆Wsoi + ∆Wsno + ∆Wcan + ∆Wa) / ∆t

P is rainfall/snowfall,

ES is soil evaporation, ET is transpiration, EC is canopy evaporation,

RSurf is surface runoff, RSub-Surf is sub-surface runoff, and

∆Wsoi / ∆t, ∆Wsno / ∆t, ∆Wcan / ∆t, and ∆Wa / ∆t are the changes in soil moisture, snow, canopy water, and aquifer water over a timestep

Main Features of the Community Land Model

• Structural aspects (surface and input datasets)

• Component submodels

Main Features of the Community Land Model

• Structural aspects (surface and input datasets)

– Heterogeneity of landscape, tiling (vegetated, urban, lake, wetland, glacier)

– Plant Functional Types and associated properties (optical, morphological, photosynthetic)

– Land cover change (changes in PFTs over time)

– Soil texture (sand, silt, clay, organic matter) and color (albedo)

– River routing

– Aerosol (snow albedo) and nitrogen deposition (CN)

Gridcell

Glacier Wetland Lake

Landunit

Columns

PFTs

Urban Vegetated

Soil Type 1

Community Land Model subgrid tiling structure

Community Land Model subgrid tiling structure

Gridcell

Glacier Wetland Lake

Landunit

Columns

PFTs

Urban Vegetated

Soil Type 1

Plant Function Type distribution in CLM4 based on MODIS/Crop datasets

Lawrence and Chase, 2007

Plant Functional Type Parameters

• Optical properties (visible and near-infrared):

– Leaf angle

– Leaf reflectance

– Stem reflectance

– Leaf transmittance

– Stem transmittance

• Land-surface models are parameter heavy!!!

• Morphological properties:

– Leaf area index (annual cycle)

– Stem area index (annual cycle)

– Leaf dimension

– Roughness length/displacement height

– Canopy height

– Root distribution

• Photosynthetic parameters:

– specific leaf area (m2 leaf area g-1 C)

– m (slope of conductance-photosynthesis relationship)

Land Use Change

Wood harvest

BET

Crop

C4 Grass

BET

Crop

C4 Grass

Land cover / land use change (prescribed)

Land cover change (prescribed)

2005 – 1850 Trees Crops

Deforestation across Eastern North America, Eastern Europe, India, China, Indonesia, SE South America for Crops

Lawrence, P et al. J. Climate, 2012

Impact of historical land cover change on climate

1976 to 2005 – 1850 to 1879

Soil Texture

Soil parameters are derived from sand / clay percentage and soil organic matter content which is specified geographically and by soil level

• Soil moisture concentration at saturation • Soil moisture concentration at wilting point • Hydraulic conductivity at saturation • Saturated soil suction • Thermal conductivity • Thermal capacity

Soil profile 10 soil levels (~3.5m) 5 bedrock levels (~50m)

River Transport Model

Raw GCM runoff Routed GCM runoff Observed riverflow

20-yr average river flow (m3 s-1)

River Discharge

River flow at outlet Top 50 rivers (km3 yr-1)

Annual discharge into Global ocean

Ac

cu

mu

late

d d

isch

arg

e fr

om

90

oN

(1

06 m

3 s

-1)

CLM3: r = 0.86 CLM3.5: r = 0.87 CLM4SP: r = 0.94 CLM4CN: r = 0.77

CLM4SP Obs CLM4CN CLM4SP CLM3.5

CLM3

Main Features of the Community Land Model • Component submodels

– Vegetation/Soil

• Hydrology (evapotranspiration, runoff, soil moisture, groundwater, river transport)

• Snow

• Soil thermodynamics

• Surface albedo and radiative fluxes

– Urban, Lake, Wetland, and Glacier

– Biogeochemistry

• Dust

• Biogenic Volatile Organic Compounds

• Carbon-Nitrogen

• Dynamic Vegetation

Land model processes - Hydrology

α, T*, zo

Rainfall Canopy evaporation

Surface runoff

Throughfall

Transpiration

Soil evaporation

Sub-surface runoff

Sublimation

Infiltration

Land model processes - Hydrology

α, T*, zo

Rainfall Canopy evaporation

Surface runoff

Throughfall

Transpiration

Soil evaporation

Sub-surface runoff

Sublimation

Stomatal conductance: solar radiation, temp, humidity deficit, soil moisture, [CO2] … Nitrogen fertilization

Photosynthesis model

Infiltration

Land model processes - Hydrology

α, T*, zo

T2, T1,

T3,

T10,

Rainfall Canopy evaporation

Surface runoff

Throughfall

Transpiration

Soil evaporation

Sub-surface runoff

Sublimation

Photosynthesis model

Runoff Vertical water flow Phase change

Soil hydrology

model

Land model processes - Hydrology

α, T*, zo

T2, T1,

T3,

T10,

Rainfall Canopy evaporation

Surface runoff

Throughfall

Transpiration

Soil evaporation

Sub-surface runoff

Sublimation

Photosynthesis model

Soil hydrology

model

Snow model

accumulation compaction melt

Modeling evaporation and runoff

“The ability of a land-surface scheme to model evaporation correctly depends crucially on its ability to model runoff correctly. The two fluxes are intricately related.”

(Koster and Milly, 1997).

Soil wetness

Eva

p, R

un

off

Runoff and evaporation vary non-linearly with soil moisture

Subgrid-scale soil moisture heterogeneity

A major control on soil moisture heterogeneity and thus runoff is topography. Lowland soils tend to be zones of high soil moisture content, while upland soils tend to be progressively drier.

Three main sources of runoff: •Infiltration excess occurs over the unsaturated fraction •Saturation excess occurs over the saturated fraction •Baseflow (drainage)

Runoff processes

Infiltration excess

P P

P

qo

Severe storms

Frozen surface Urban area

SIMTOP: Simple TOPMODEL-based runoff model

Niu et al. 2005

Subgrid-scale soil moisture heterogeneity

Infiltration excess

P P

P

qo

Severe storms

Frozen surface Urban area

SIMTOP: Simple TOPMODEL-based runoff model

Saturation excess

P P

P

qr qs

qo zwt

Niu et al. 2005

( ) ( ),1 max ,11 exp 0.5sat frz over wt frzf f f f z f= − − +

Groundwater model (SIMGM) determines water table depth

Subsurface runoff is exponential function of water table depth

Niu et al. 2007

Groundwater in CLM

Groundwater controls runoff (Yeh and Eltahir, 2005)

Groundwater affects soil moisture and ET (Gutowski et

al, 2002; York et al., 2002)

water table

Yeh and Eltahir, 2005

GW level (m)

Str

ea

mfl

ow

(m

m/m

on

)

Precipitation (mm/mon)

Soil (and snow) water storage (MAM − SON)

300 200 100 0 -100 -200 -300 (mm)

CCSM3

CCSM4 GRACE (obs)

GRACE satellite measures small changes in gravity which on seasonal timescales are due to variations in water storage CCSM3 and CCSM4 data from 1870 and 1850 control

Abracos tower site (Amazon)

CLM3

Latent Heat Flux

OBS

Mod

el

CLM3.5/4 CLM3

Total soil water

CLM3.5/4

Latent Heat Flux

OBS

Mod

el

Sn

ow

de

pth

Tsnow

Model components: Snow Model

• Up to 5-layers of varying thickness

• Treats processes such as

• Accumulation

• Snow melt and refreezing

• Snow aging

• Water transfer across layers

• Snow compaction

• destructive metamorphism due to wind

• overburden

• melt-freeze cycles

• Sublimation

• Aerosol deposition

Snow, Ice, and Aerosol Radiative Model (SNICAR)

– Snow darkening from deposited black carbon, mineral dust, and

organic matter – Vertically-resolved solar heating in the snowpack – Snow aging (evolution of effective grain size) based on:

• Snow temperature and temperature gradient • Snow density • Liquid water content and • Melt/freeze cycling

Flanner et al (2007), JGR Flanner and Zender (2006), JGR Flanner and Zender (2005), GRL

Snow cover fraction

How much of a grid cell is covered with snow for a given snow depth?

Niu and Yang 2007

Snow/Soil thermodynamics

Solve the heat diffusion equation for multi-layer snow and soil model

∂∂

∂∂

=∂∂

zTK

ztTCp

where Cp (heat capacity) and K (thermal conductivity) are functions of:

• temperature

• total soil moisture

• soil texture

• ice/liquid content

Modeling Permafrost in CLM

Lawrence et al., J. Climate, 2011

Modeling surface albedo

Surface albedo a function of

– Vegetation cover and type

– Snow cover

– Snow age

– Solar zenith angle

– Soil moisture

– Amount of direct vs diffuse solar radiation

– Amount of visible vs IR solar radiation

Surface albedo (CLM offline compared to MODIS)

Bias (%) RMSE (%)

Model Snow-free

Snow depth> 0.2m

Snow-free

Snow depth >

0.2m

CLM3.5 2.7 -5.0 4.1 11.9

CLM4SP 0.4 2.9 2.0 13.2

Note: MODIS albedo biased low for snow at high zenith angle (Wang and Zender, 2010)

CLM near-term development activities

– Crops and irrigation

– Revised cold region hydrology

– Revised canopy processes (radiation and photosynthesis)

– Methane emissions model

– Improved fire algorithm including human triggers and suppression

– Revised lake model

– High spatial resolution input datasets

– Multiple urban density types, improved anthropogenic fluxes

Thank You

The NESL Mission is: To advance understanding of weather, climate, atmospheric composition and processes;

To provide facility support to the wider community; and, To apply the results to benefit society.

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NCAR is sponsored by the National Science Foundation